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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-12865-2011</article-id>
<title-group>
<article-title>Growth rates of nucleation mode particles in HyytiÃ¤lÃ¤ during 2003&amp;minus;2009: variation with particle size, season, data analysis method and ambient conditions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yli-Juuti</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nieminen</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hirsikko</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Aalto</surname>
<given-names>P. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Asmi</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>HÃµrrak</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Manninen</surname>
<given-names>H. E.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Patokoski</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dal Maso</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>PetÃ¤jÃ¤</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rinne</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kulmala</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Riipinen</surname>
<given-names>I.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Physics, University of Helsinki, P.O. Box 64, 00014, University of Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Finnish Meteorological Institute, Erik PalmÃ©nin aukio 1, 00560 Helsinki, Finland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Institute of Physics, University of Tartu, Ãœlikooli 18, 50090 Tartu, Estonia</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Applied Environmental Science and Bert Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>12</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>24</issue>
<fpage>12865</fpage>
<lpage>12886</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/12865/2011/acp-11-12865-2011.html">This article is available from http://www.atmos-chem-phys.net/11/12865/2011/acp-11-12865-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/12865/2011/acp-11-12865-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/12865/2011/acp-11-12865-2011.pdf</self-uri>
<abstract>
<p>The condensational growth rate of aerosol particles formed in atmospheric
new particle formation events is one of the most important factors
influencing the lifetime of these particles and their ability to become
climatically relevant. Diameter growth rates (GR) of nucleation mode
particles were studied based on almost 7 yr of data measured during the
years 2003â€“2009 at a boreal forest measurement station SMEAR II in
HyytiÃ¤lÃ¤, Finland. The particle growth rates were estimated using
particle size distributions measured with a Differential Mobility Particle
Sizer (DMPS), a Balanced Scanning Mobility Analyzer (BSMA) and an Air Ion
Spectrometer (AIS). Two GR analysis methods were tested. The particle growth
rates were also compared to an extensive set of ambient meteorological
parameters and trace gas concentrations to investigate the
processes/constituents limiting the aerosol growth. The median growth rates
of particles in the nucleation mode size ranges with diameters of 1.5â€“3 nm,
3â€“7 nm and 7â€“20 nm were 1.9 nm h&lt;sup&gt;âˆ’1&lt;/sup&gt;, 3.8 nm h&lt;sup&gt;âˆ’1&lt;/sup&gt;, and 4.3 nm h&lt;sup&gt;âˆ’1&lt;/sup&gt;,
respectively. The median relative uncertainties in the growth
rates due to the size distribution instrumentation in these size ranges were
25%, 19%, and 8%, respectively. For the smallest particles
(1.5â€“3 nm) the AIS data yielded on average higher growth rate values than
the BSMA data, and higher growth rates were obtained from positively charged
size distributions as compared with negatively charged particles. For
particles larger than 3 nm in diameter no such systematic differences were
found. For these particles the uncertainty in the growth rate related to the
analysis method, with relative uncertainty of 16%, was similar to that
related to the instruments. The growth rates of 7â€“20 nm particles showed
positive correlation with monoterpene concentrations and their oxidation rate by
ozone. The oxidation rate by OH did not show a connection with GR. Our
results indicate that the growth of nucleation mode particles in
HyytiÃ¤lÃ¤ is mainly limited by the concentrations of organic
precursors.</p>
</abstract>
<counts><page-count count="22"/></counts>
</article-meta>
</front>
<body/>
<back>
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